- 责任者：Wu Xiaozhi (China University of Geosciences ; Beijing 100083 ; China) ; Lang Fengjiang
- 刊名：Chinese Journal of Geology
- 出版年：2011
- 卷期：46(3)
- 关键词：油气聚集 ; oil and gas accumulation ; 构造演化 ; structural evolution ; 新疆 ; Xinjiang
- 页码：p.808-825
- 图表：8 illus., 21 refs.
- 分类号：1003
- 出版序号：696
- issnNo：ISSN0563-5020
- isbnNo：CN11-1937/P
Santanghu Basin is in the southern rim of the Siberia Plate. Its evolution was composed by the following tectonic activity: ocean crust extinction, fault depression shrinkage and basin uplifting, formed erosion unconformity. Basin was divided into three structural belts: east northern thrust nappe uplift, central depression and west southern thrust nappe belt. There are three types of hydrocarbon accumulation: accumulated in the north eastern depression uplift and paleo-uplift, in the north western thrust fault belt, in the unconformity. The petroleum source of Santanghu Basin was up to 7×108 -9×108t. It has a low exploration degree. There are four exploration potentials: shallow Jurassic litho-stratigraphic reservoir surrounding Malang-Tiaohu depression, Carboniferous volcanic weathering crust reservoir in the northern uplift, Permian dolomite and Carboniferous volcanic reservoir in the southern thrust nappe belt.